Early to mid-Pleistocene ostracod δ18O and δ13C in the central Tibetan Plateau: Implication for Indian monsoon change

Palaeogeography, Palaeoclimatology, Palaeoecology

Volumn 280, Issue 3-4, 2009, Pages 406-414

  Jin, Zhangdong ^a   Bickle, Mike J ^b   Chapman, Hazel J ^b   Yu, Jimin ^c   Wang, Sumin ^d   Chen, Shiyue ^e  

^a Chinese Academy of Sciences   (China)

^b UNIVERSITY OF CAMBRIDGE   (United Kingdom)

^c International Research Institute for Climate and Society   (United States)

^d NANJING INSTITUTE OF GEOGRAPHY AND LIMNOLOGY   (China)

^e LIAOCHENG UNIVERSITY   (China)

Author keywords

Central Tibetan Plateau; Indian monsoon; Lake sediment; Ostracod shell; Stable isotopes

Indexed keywords

CORE ANALYSIS; LACUSTRINE DEPOSIT; LAKE WATER; MONSOON; OSTRACOD; PLATEAU; PLEISTOCENE;

ASIA; CHINA; EURASIA; FAR EAST; QINGHAI-XIZANG PLATEAU;

OSTRACODA;

EID: 69049097992     PISSN: 00310182     EISSN: None     Source Type: Journal    
DOI: 10.1016/j.palaeo.2009.06.028     Document Type: Article

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